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Index to Marine and Lacustrine Geological Samples (IMLGS)

Repository: Lamont-Doherty Earth Observatory
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Ship: Vema
Cruise: VM34 (V3407)
Sample: 084
Device: core, piston
Latitude: 11.567
Longitude: 57.93
Water Depth(m): 4744
Date: 19770905
IGSN: DSR000CX1
Core length (cm): 997
Diameter (cm): 6
Storage: room temperature, dry
1 :    0 to 8 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
Components: calcareous, biogenic
siliceous
2 :    8 to 29 cm in core
Primary composition: calcareous, biogenic
Primary texture: sandy mud or ooze
3 :    29 to 38 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
Components: siliceous
4 :    38 to 43 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
5 :    43 to 99 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
Components: calcareous, biogenic
6 :    99 to 109 cm in core
Primary composition: siliceous, diatoms
Primary texture: mud or ooze
Components: siliceous, sponge spicules
calcareous, nannofossils
7 :    109 to 190 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
Components: siliceous
8 :    190 to 200 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
9 :    200 to 233 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
10 :    233 to 365 cm in core
Primary composition: siliceous, diatoms
Primary texture: sandy mud or ooze
Components: calcareous, nannofossils
11 :    365 to 430 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
Components: calcareous, foraminifera
12 :    430 to 997 cm in core
Primary composition: calcareous, nannofossils
Primary texture: sandy mud or ooze
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When you refer to individual samples/data in the IMLGS, please cite each source repository whose data you use.

More Information and how to cite the IMLGS: doi:10.7289/V5H41PB8.


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